Explanation:
The Northeast Monsoon blows from the land (the Asian mainland) to the sea (Bay of Bengal) during the winter months (October to December), bringing rainfall to southern India.
Explanation:
The heating of the Tibetan Plateau during pre-monsoon season creates a large thermal low, drawing in moisture-laden winds from the Indian Ocean, triggering the monsoon.
Explanation:
The 'Loo' is a strong, hot, and dry summer wind that blows over the northern plains of India, particularly in the states of Bihar, Uttar Pradesh, and Rajasthan.
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